Etude geophysique des dorsales de l'ocean Indien dans la region du point triple de Rodriguez

Autre(s) titre(s) Geophysical study of the Indian Ocean spreading ridges close to the Rodriguez Triple Junction
Type Article
Date 1990
Langue(s) Français
Auteur(s) Munschy M, Schlich R
Conférence Actes du Colloque Tour du monde Jean Charcot , Paris (France), 2-3 Mar 1989
Source Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1990
Résumé en anglais The Indian Ocean is dominated by as system of 3 mid-ocean ridges converging at the Rodriguez Triple Junction located near 25 degree 30'S and 70 degree E. Numerous studies carried out on these 3 ridges provided the basic information on spreading rates and spreading directions. In 1984 the R/V Jean Charcot conducted a detailed survey over the Rodriguez Triple Junction and over an axial ridge segment located on each of the 3 associated ridges. The ridge axes are cut by distinct rift valleys; the depth of these rift valleys is a function of spreading rates. The rift valleys are not in isostatic equilibrium, but show clear density and mass deficits (0.4 to 0.8 g.cm super(-3) for spreading rate of 1 cm/a and 0.1 to 0.3 g.cm super(-3) for spreading rates of 3 cm/a). The Rodriguez Triple Junction is unstable. The axis of the Central Indian Ridge is offset from the axis of the Southeast Indian Ridge at a velocity of 0.14 cm/a.
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Munschy M, Schlich R (1990). Etude geophysique des dorsales de l'ocean Indien dans la region du point triple de Rodriguez. Oceanologica Acta, Special issue Open Access version : https://archimer.ifremer.fr/doc/00268/37894/